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Article

Assessment of Heavy Metal Pollution in the Sediment of the Main Tributaries of Dongting Lake, China

1
State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China
2
University of Chinese Academy of Sciences, Beijing 100049, China
*
Author to whom correspondence should be addressed.
Water 2018, 10(8), 1060; https://doi.org/10.3390/w10081060
Submission received: 13 July 2018 / Revised: 1 August 2018 / Accepted: 6 August 2018 / Published: 10 August 2018
(This article belongs to the Section Water Quality and Contamination)

Abstract

:
Heavy metal pollution in sediment is one of the most serious problems in water bodies, including rivers, which can cause secondary pollution when environmental conditions change. In this study, surface sediment samples collected from the four main tributaries of Dongting Lake (i.e., Xiangjiang River (XR), Zishui River (ZR), Yuanjiang River (YR), and Lishui River (LR)) were analyzed for concentrations of Zn, Cr, Cu, As, Cd, and Pb. The spatial distribution, source, and potential ecological risk of these metals were determined. The results suggest a great spatial heterogeneity of heavy metals in the sediment of the studied rivers. Heavy metals had highest concentrations in the sediment of XR, especially midstream and downstream. A principal component analysis (PCA) and correlation analysis indicated that Cd and As were mainly from industrial wastewater and mineral mining, Cr came from natural process and agricultural activities, and Zn and Cu potentially from both. Pb was originated from atmospheric deposition and river inflow transportation. According to the geo-accumulation index ( I g e o ), enrichment factor (EF), and risk index (RI) assessment, heavy metals pollution was highest in the sediment of XR, and Cd was the main pollutant in the sediment of XR, presenting considerable potential ecological risk. This may contribute to heavy metal pollution in Dongting Lake. This paper provides a reference for the aquatic environmental management of heavy metals in Dongting Lake area and its tributaries.

1. Introduction

Aquatic systems enable hydrological cycling, climate regulation, and habitat provision for aquatic organisms. Heavy metal pollution in the aquatic environment has attracted global attention because of the environmental toxicity, persistence, and bioaccumulation of heavy metals, which can pose adverse effects on living beings and the entire ecosystem [1,2]. Sediment is considered as the largest pool of heavy metals in the aquatic environment [3,4]. About 99% of the heavy metals load in aquatic systems has been found to ultimately precipitate onto the sediment [5]. Heavy metal concentrations in the sediment are usually four or five times higher than that found in the overlying water [6]. Thus, sediment quality can reflect the heavy metal pollution status of the whole ecosystem. Consequently, it is of great importance to measure the amount of heavy metals in the sediment to provide information on the heavy metal contamination of the entire aquatic ecosystem.
Heavy metals enter aquatic ecosystem sediment via natural processes, including atmosphere deposition, rock weathering and erosion, and hydrodynamic alteration, as well as via anthropogenic activities, such as industrial wastewater discharge and agricultural fertilizer leaching [7]. With the rapid development of industrialization, urbanization, and agriculture, anthropogenic activities have become the main source of heavy metal pollution in the sediment of many rivers around the world. When the environmental factors of pH, oxidation-reduction potential (Eh), and organic matter [7,8,9] change, the heavy metal in sediment may release into the overlying water. In addition, the flushing operation caused by flow may not only cause the resuspension of sediment, but also affect the spatial distribution of heavy metals in the sediment [10]. As well as the artificial replenishing activities of sediment that may result in the dispersion of pollutants (include heavy metals) in the sediment [11,12]. Accordingly, it is required to have a comprehensive assessment of the sediment quality, considering environmental changes.
Various studies have focused on the assessment of the extent of metal pollution using numerous analytical techniques based on heavy metal concentration and distribution patterns [13,14,15]. Ke et al. [16] assessed the ecological risk of the heavy metals Cd, As, Cu, Ni, Pb, Cr, and Zn, with sediment quality guidelines (SQGs), geo-accumulation index ( I g e o ), potential ecological risk index (RI), and risk assessment code (RAC). Zahra et al. [9] determined the metal accumulation, distribution, and pollution status using the enrichment factor (EF), I g e o , and metal pollution index (MPI) of the Rawal Lake tributary. EF and I g e o take into consideration the enrichment and pollution status of a single element; RI, SQG, and MPI take into consideration the combined effects of heavy metals, while RAC is mainly used to determine the speciation effect of heavy metals. Therefore, it is essential to determine the values of several combined indices for a comprehensive understanding of heavy metal pollution in the sediment.
Located south of the middle reaches of the Yangtze River, Dongting Lake is the second largest freshwater lake in China and has the Xiangjiang River (XR), Zishui River (ZR), Yuanjiang River (YR), and Lishui River (LR) as its main feeding tributaries [17]. The lake serves more than 600 million inhabitants and plays an important role in providing food and habitats for living beings, maintaining biodiversity, and controlling flooding [18]. Frequent mining and agricultural cultivation along the four tributaries have made them the primary source of heavy metals in Dongting Lake [19]. Presently, numerous studies have been conducted to evaluate the toxicity and ecological risk of heavy metals in the main body of Dongting Lake or part of its tributaries [17,20,21]. Nevertheless, there have been only a limited number of studies performed on a comprehensive comparison between the heavy metals in the sediments of the major tributaries listed above. Tributary rivers are the main source of pollutants for a lake and play an important role in maintaining a healthy lake ecosystem [9,22]. Therefore, this study is a comprehensive evaluation of heavy metals in the sediment of the four feeding tributary rivers in order to enable the efficient management of heavy metal pollution in Dongting Lake and its tributaries.
Given the importance of heavy metal pollution in sediment, this study was devoted to the analysis of the contamination of heavy metals (Zn, Cr, Cd, Pb, As, and Cu). The primary objectives of this study are as follows: (1) to investigate the spatial distribution of heavy metals in the surface sediment of the four tributaries by comparing them with various background values and previous studies; (2) to assess the level of contamination and potential ecological risk of heavy metals in sediments of the four tributaries using EF, I g e o , and RI; and (3) to explore the possible sources of heavy metals in the sediment of the four tributaries using correlation analysis and principal component analysis (PCA).

2. Materials and Methods

2.1. Study Area

Dongting Lake (28°44′–29°35′ N, 111°53′–113°05′ E), the second largest freshwater lake in China, is located south of the middle reaches of the Yangtze River, and is strongly affected by the East Asian monsoon (Figure 1) [23]. The mean annual temperature is 16.4–7.0 °C in the Dongting Lake area and the mean annual precipitation in the area is 1100–1400 mm/year, but the precipitation is mainly concentrated from April to June. Dongting Lake receives water mainly from the four tributaries, namely XR, ZR, YR, and LR, and then water flows into the Yangtze River at Chenglingji. The four tributaries, covering a drainage area of about 23.5 km2 [7], contribute about 68.3% of the runoff volume and 20% of the sediments of the Dongting Lake (Bulletin of the Yangtze River Sediments, 2006–2016). Previous studies have suggested that the four tributaries are polluted by heavy metals, with anthropogenic activities in their local environment as the main source responsible for pollutants [17,24,25].

2.2. Sample Collection

Superficial sediment samples (0–10 cm) were collected in April (dry season) and in July (wet season) from upstream, midstream, and downstream portions of the four tributaries, in order to provide good area coverage (Figure 1). A composite surface sample (about 200 g) at each site was collected because it is more chemically and biologically active than the deep layers, and more benthic organisms occupied this layer [16]. At each site, three samples were collected using a portable Ekman grab sampler, and were subsequently well mixed in situ, then placed in an acid-rinsed polyethylene plastic bag and sealed. The sediment samples were kept at 4 °C while being transferred to the laboratory for processing.

2.3. Chemical Analysis

The analysis of the heavy metal concentration was performed at the State Key Laboratory of Nanjing Institute of Geography and Limnology, The Chinese Academy of Science. The sediment samples were freeze-dried and homogenized by grinding, using an agate mortar and pestle to pass through an 100 mesh nylon sieve at room temperature. The samples (0.5 g) were then digested in 20 mL of a 1:1:2 guaranteed reagent HNO3 + HClO4 + HF in the Milestone ETHOS ONE digestion system for 10 h. The digested samples were filtered (0.45 μm filter membrane) and adjusted to a suitable volume. The total concentrations of Cr, Cu, Zn, Pb, Cd, and As were analyzed using inductively coupled plasma-mass spectrometry (ICP-MS, 7700x, NYSE: A, America). The quality assurance and quality control of the analytical data were assessed in duplicate, with method blanks and standard reference materials. Three replicates were conducted for the determination of the total content of each heavy metal, and the total content of each heavy metal was expressed as the mean concentration of the replicates. The results were consistent with the reference values (Chinese national geo-standard [GBW-07333 and GBW-07314]), the differences of duplicated samples were within ±10%, and the measurement errors between the determined and certified values were less than 5%.
All of the reagents were of supra quality and of analytical grade, and all of the solutions were prepared using ultra-pure water. All of the glassware and plastic were pre-cleaned by soaking in HNO3 (10%) for at least 48 h, then rinsed repeatedly with ultra-pure water.

2.4. Statistic Analysis

An analysis of variance (ANOVA) was performed to assess the mean differences of the studied parameters among the rivers. A correlation analysis was conducted to ascertain whether or not a combined contamination among the heavy metals exists. The principal component analysis (PCA) is as an unsupervised pattern recognition method with varimax rotation and Kaiser normalization, which is widely used to reduce the related random environmental variables and to extract a small set of distinct variables (principal components [PCs]) that account for a large proportion of the total variance in the data. The non-normal data was transformed to normality using a logarithm or square root. Prior to PCA, the Kaiser–Meyer–Olkin (KMO) and Bartlett’s sphericity tests were used to evaluate the validity of the original data, requiring that the KMO values should be more than 0.5 and that the Bartlett’s sphericity tests be significant (p < 0.0001). The PCs with eigenvalues >1 were retained. All of the statistical analyses were conducted with R language software and all of the statistical methods were performed with a 95% confidence at p < 0.05.

2.5. Metal Assessment in Sediment

The background value is of great importance in estimating the pollution degree and potential ecological risk of heavy metals in sediments. The shale and average crustal abundance data were typically used as background values [26]. In this paper, EF, I g e o , and RI were calculated to estimate the contamination degree of the heavy metals in the surface sediment of the four rivers. Considering the regional discrepancies, the sediment background value of the heavy metals in the Dongting Lake drainage area was selected as the background value against which to evaluate the heavy metal pollution in the sediments of the four rivers [27].

2.5.1. Calculation of Enrichment factor (EF)

The EF was calculated to estimate the enrichment and possible anthropogenic impact of heavy metals on sediments using the following equation [9]:
  EF = ( C i / C F e ) S e d i m e n t ( C i / C F e ) B a c k g r o u n d  
where ( C i / C F e ) S e d i m e n t is the ratio of the concentration of a particular metal ‘ i ’ ( C i ) to the Fe concentration C F e in the sediment sample; and ( C i / C F e ) B a c k g r o u n d is the ratio of the background concentration of a particular metal ‘ i ’ ( C i ) to the reference background concentration of Fe ( C F e ), which is mainly used to decrease the influence of particle grain size on heavy metal contamination measurement.

2.5.2. Calculation of Geo-Accumulation Index ( I g e o )

The contamination caused by heavy metals in sediment can be assessed by I g e o [28], as follows:
  I g e o = log 2 [ C i 1.5 B i ]  
where I g e o is the concentration of the measured heavy metal i , and B i is the geochemical background concentration of metal i . The corresponding background concentration of the heavy metals in the sediment of Dongting Lake [27] were used as B i in this paper. The factor 1.5 corresponds to the possible variation of the crustal contribution to sediment, mainly by weathering or erosion in the rivers.

2.5.3. Calculation of Potential Ecological Risk (RI)

RI was used to assess the potential ecological risk of heavy metal to the aquatic ecosystem, considering the toxicity and combined effects of each heavy metal, which EF and I g e o do not take into account. The calculation of the contamination factor ( C f i ) and ecological risk factor ( E i ) of each heavy metal is the first step toward determining the RI. The following are the equations to measure C f i and E r i , respectively:
  C f i = C i / C b i  
  E r i = C f i · T r i  
where C i is the concentration of heavy metal i in the sediment sample, and C b i and T r i are the preindustrial background value and toxic response factor in the sediment, respectively, obtained from the literature [29].
The RI was established by summing the E r i of each heavy metal, as follows:
  RI = E r i  
The classes of EF, I g e o , and RI are listed in Table 1.

3. Results

3.1. Spatial Distribution of Heavy Metals

The mean concentration of the heavy metals followed a decreasing ranking order of Zn–Pb–Cr–Cu–As–Cd, with values of 197 mg/kg for Zn, 71 mg/kg for Pb, 66 mg/kg for Cr, 42 mg/kg for Cu, 38 mg/kg for As, and 5.85 mg/kg for Cd (Table 2). All of the metals’ concentration varied significantly among the rivers (p < 0.05), except Cr (Figure 2). The Zn, Cu, and As concentrations were highest in XR (374.45 mg/kg, 65.85 mg/kg and 84.70 mg/kg), followed by ZR (187.37 mg/kg, 40.11 mg/kg and 30.59 mg/kg), YR (149.64 mg/kg, 37.50 mg/kg and 24.54 mg/kg), and LR (78.42 mg/kg, 24.19 mg/kg and 13.93 mg/kg). While the Cr, Cd, and Pb concentrations descended in the order of XR–YR–ZR–LR, with the highest concentrations of 87.31 mg/kg, 14.30 mg/kg, and 106.08 mg/kg in XR, respectively.
The heavy metals in the sediment of different sections of the rivers were not regularly distributed (Figure 3). In XR, all of the metals, except Cr, had higher concentrations in the midstream and downstream regions, especially As and Cd. The As concentrations in the midstream (113.42 mg/kg) and downstream (111.77 mg/kg) were more than 3.5 times higher than the concentrations upstream (28.90 mg/kg). The Cd values in the midstream (22.04 mg/kg) and downstream (18.84 mg/kg) regions were more than 11- and 9-fold higher than the upstream (2.02 mg/kg), respectively. The heavy metals were also present at a higher concentration midstream and downstream of LR, with the exception of Cd, which had significantly higher values upstream (6.00 mg/kg). The Zn, As, and Cd concentrations in ZR and YR, as well as the Cr concentration in ZR, were higher in the midstream and downstream regions. The Pb concentration was significantly higher in the upstream of YR and midstream of ZR, while the Cu and Cr concentrations in YR were higher in the midstream region.
The mean concentrations of Cd, Pb, As, Zn, Cu, and Cr were significantly higher than the background value of the Dongting Lake sediment, respectively, as well as the upper continental crust (UCC) values and the freshwater sediment screening benchmarks of the US EPA (United States Environmental Protection Agency), and the threshold effects level (TEL) (Table 2). Only the average concentration of Cd was more than 7.6 times higher than the probable effects level (PEL). In comparison with the concentrations of heavy metals reported in the sediments in other rivers in China and other countries, the As, Cd, and Pb concentration in the present study exceeded all of the the rivers, except that Pb was relatively lower than that in the sediment of the Tigris River; the Zn, Cu, and Cr concentrations were higher than some of the reported rivers.

3.2. Risk Assessment of Heavy Metals

To ascertain the degree of contamination and the possible sources (natural and anthropogenic sources) of heavy metals (Zn, Cr, Cu, As, Pb, and Cd), EF, I g e o , and RI were established. Table 3 presents the EF values of heavy metals in the sediment. The mean EF values for Cd (14.24) were >10, while the other metals were in the range of 1–3. All of the EF values for Cd in the sediments of the four rivers were significantly higher than 1 and in the order of EF (XR) = 33.58 > EF (YR) = 9.03 > EF (ZR) = 7.77 > EF (LR) = 6.57. These values indicate an extremely severe enrichment of Cd in XR, and a severe enrichment of Cd in the other three rivers. The EF values for Cd were especially high in the midstream and downstream regions of XR (54.26 and 42.06, respectively) and ZR (10.34 and 10.40, respectively), in addition to the midstream region of YR (17.83) and the upstream region of LR (15.79). In addition, XR had the highest EF values of As, in the range of 5–10, and Zn, in the range of 3–5, especially common in the midstream and downstream regions, indicating a moderately severe enrichment and moderate enrichment of these two metals, respectively. Cu and Cr had highest EF values in XR in the range of 1–3, while Pb had the highest EF values in YR (4.09), especially in the upstream region (8.87).
In a similar pattern to the established EF values, Cd had the highest mean I g e o value (2.31) compared with other metals, suggesting moderate to high levels of pollution in the river sediment (Table 4). Other metals had I g e o values of <1 or <0, indicating an absence of pollution or minor levels of pollution in the sediment. The Cd I g e o values in the sediment of the four rivers can be ranked in order of XR ( I g e o = 4.14 ) > ZR ( I g e o = 2.31 ) > YR ( I g e o = 1.86 ) > LR ( I g e o = 0.91 ). This indicates a high to very high pollution of XR sediment, and un-polluted to minor pollution levels in other river sediments by Cd. Moreover, Cd had a relatively higher I g e o value in the sediment of the midstream and downstream regions of XR ( I g e o = 5.21, 5.20, respectively) and ZR ( I g e o = 2.85, 3.09, respectively), the midstream region of YR ( I g e o = 3.94), and the upstream region of LR ( I g e o = 2.21), as compared with other sections of rivers. The I g e o values for As were also the highest in XR (1.74), especially in the midstream ( I g e o = 2.55 ) and downstream ( I g e o = 2.50 ) regions.
Table 5 shows the ecological risk factor E r i of the individual heavy metals, and the potential ecological risk index (RI) of the combined heavy metals present in the sediments of the four rivers. The mean E r i values of Zn, Cr, Cu, and Pb were smaller than 40, except Cd ( E r i =   175.64), suggesting a low ecological risk from these metals. Cd had highest E r i values in the sediment of XR ( E r i = 428.95), followed by YR ( E r i =   111.69), ZR ( E r i   =   89.75), and LR ( E r i =   72.18). The E r i values were particularly higher in the midstream and downstream region of XR ( E r i   =   661.18, 565.21, respectively) and ZR ( E r i   =   109.82, 126.79, respectively), in the midstream region of YR ( E r i   =   228.36), and upstream of LR ( E r i   =   179.97), than in other sections of the respective rivers. The metals in the sediment of all of the rivers present a low potential ecological risk, except for at XR (RI = 503.66), where they pose a considerable potential ecological risk. The potential ecological risk index values indicated that the metals in the sediment caused moderate potential ecological risk (RI = 213.097) overall.

3.3. Source Identification for Heavy Metal Pollutants

The correlation among heavy metals may indicate the same source and similar migration pattern of these elements [16]. The lack of any significant correlation signifies that the heavy metals may originate from different sources and be controlled by multiple factors. The Pearson correlation of the analyzed metals is presented in Table 6. Zn, Cr, Cu, As, and Cd were significantly correlated with each other (For example: Zn–Cr: r = 0.548, p < 0.05; Zn–Cu: r = 0.779, p < 0.05; Zn–As: r = 0.772, p < 0.05; Zn–Cd: r = 0.785, p < 0.05; Cr–Cu: r = 0.745, p < 0.05), with the exception of Cr, which was not significantly correlated with either As or Cd. Moreover, Pb was not significantly correlated with any metals, except Cr (r = 0.456, p < 0.05).
To clarify the origin of the heavy metals in the studied area, PCA was chosen as the analysis tool. Table 7 shows the component matrix and variance of the metals in the studied rivers extracted by eigenvalue >1. Figure 4 shows the variation diagram in rotated space with the first two components as axes. Two components were extracted, explaining 81.946% of the total variance, which is therefore in accordance with the regulation that the principal components should account for at least 75% of the total variance [40]. Component 1 showed the general loading of surface sediments with heavy metals. It was heavily loaded with Cd, As, and Zn, while being moderately loaded with Cu, explaining 58.85% of the total variance with an eigenvalue of 3.531. Component 2 explained 23.09% of the total variance, having a high positive loading with Cr, Cu, and Pb, and moderately loading with Zn.

4. Discussion

Heavy metals are a special group that may mainly be derived from anthropogenic activities, with some contribution from natural sources [41]. In the present study, concentrations of Zn, Cu, As, Cd, and Pb were significantly higher in XR than other rivers, while significantly lower in LR than other rivers, especially in the midstream and downstream regions of the two rivers. These results indicate that heavy metals in the sediment of the four rivers had a high degree of spatial heterogeneity. Taking the similarity in climate and background values of these rivers into consideration, anthropogenic activities, such as urbanization, industry, agriculture, aquaculture, and tourism development, may be main factors in the spatial differences in the heavy metal concentrations in the sediment [42]. Hunan Province is rich in non-ferrous metals, with high levels of mining, mineral processing, and smelting, contributing to the high concentrations distributed in the midstream and downstream region of XR [18,43,44,45]. In addition, many large cities, such as Xiangtan, Zhuzhou, and Changsha, are also located in the midstream and downstream regions of XR [46]. This urbanization and mineral utilization might explain the high concentration of heavy metals in the sediment of XR. Moreover, the large drainage area of XR may bring non-point source pollutants [47]. The construction of a dam in the upstream may enhance the flushing of the river [48], and this may also contribute to the relatively higher heavy metal concentrations in the middle and lower reaches of XR. While the phosphorous chemical production in the upstream region of YR might contribute to the significantly higher Pb concentrations observed, as compared with other sections.
The criteria for heavy metal values in the sediments have been developed by international and national governments, to assess their pollution level and ensure sediment security. In the present study, the concentrations of Zn, Cd, Pb, As, Zn, Cu, and Cr were higher than the UCC, US EPA, TEL, and background value for Dongting Lake sediment. This finding indicates that heavy metals in the sediment might cause adverse effects on the river systems studied. This was corresponded with previous studies that reported serious levels of heavy metal pollution in the sediment of Dongting Lake and its tributaries [21,49,50,51,52]. This was especially true for Cd, which was 60-fold higher than the UCC and US EPA guidelines and 7.6-fold higher than the PEL. It is of note that Hunan Province had the highest ranked level of production of Cd, As, Cr, and Pb in China for many years, as well as the highest relative industrial discharge via wastewater [17]. Furthermore, about 1.7 million tons of fertilizer and pesticides containing Cd, Cr, Pb, As, and other metals, are used annually in the Dongting Lake drainage region [53]. Therefore, anthropogenic activities surrounding the studied area might be the main reason for the heavy metal pollution in the sediment.
Heavy metal pollution of the surface sediment has been one of the most serious problems facing the Dongting Lake. Ma et al. [54] assessed heavy metals in the sediment of the six major freshwater lakes in China, namely Dongting Lake, Poyang Lake, Hongze Lake, Chaohu Lake, Taihu Lake, and Hongsi Lake, and the results indicated that Dongting Lake shows the highest ecological risk. Some studies compared the heavy metal concentration in the sediment of Dongting lake and the river inlets, the results indicated that the heavy metal concentration in the sediment of the inlet of the four rivers is higher than other parts of Dongting Lake [55]. In this study, the mean concentration of Zn, Pb, Cd, and As were higher than those found in Dongting Lake [21]. These results suggested that the four rivers may be the main sources of heavy metals in the sediment of Dongting Lake. However, the relatively lower metal concentration at the outlet of Chenglingji indicates that the metals that have flown in from rivers are diluted in the Dongting Lake [56]. The construction of The Three Gorge Dam decreases the sand contribution of Yangtze River to Dongting Lake, and increases the flushing of the Dongting Lake sediment, this may resuspend the sediment into the overlying water, thus decreasing heavy metal contents in the sediment of Dongting Lake [48].
In this study, Cd had high EF (>10), Igeo (>2), and E r i (>150) values compared with other metals, indicating that the Cd pollution levels were moderate to high in river sediments and presents a high ecological risk. This corresponds with previous reports that Cd was the main pollutants of all of the heavy metals, and had the highest ecological risk in the sediment of Dongting Lake area [21,50,52]. The Cd in the sediment of the Dongting Lake drainage is mainly in exchangeable and carbonate form, this may contribute to the high ecological risk [50,51,57]. What is more, the sensitivity of Cd to low pH, Eh, and OM (organic matter), may also partly contribute to its high ecological risk in the sediment of studied rivers [57]. This needs further validation in future study. The RI values for heavy metals in sediments indicate that heavy metals present a considerable ecological risk in XR (RI >300), while they pose a low ecological risk in the other three rivers (RI <150). This was corresponding with the high ecological risk of heavy metals in the sediment of southern and eastern Dongting Lake, while a low ecological risk of western Dongting Lake [56]. Furthermore, the significantly higher EF (>25), I g e o (>4), and E r i (>150) values indicate that Cd contributed the most to the high ecological risk of sediments in XR, especially in the midstream and downstream regions. Considering the severe toxicity caused by Cd to the respiratory system, nervous system, immune system, and DNA [58], special measures are urgently needed to control both point and non-point pollutants, and to ensure the safety of aquatic ecosystem, especially XR.
Using the correlation and PCA analysis, pairs of heavy metals were correlated with each other, with As and Cd, and Cr and Pb, presenting similar variations, respectively, suggesting a high level of consistency in their sources. Furthermore, Cu and Zn were significantly correlated with As, Cd, and Cr, as well as having a high loading in both the first and second components. This suggested that Zn and Cu originated from a mutual source to Cr, As, and Cd. The mean concentrations of Cd and As were 17.7- and 3.0-fold higher than the background value of the Dongting Lake sediment, respectively, indicating an anthropogenic source for the two metals. This is corroborated by the moderate to high levels of Cd pollution, while the As pollution was absent to moderate, as derived by the assessment of EF and I g e o . According to the Hunan Statistical Year Book (2017), the content of Cd and As in the sewage discharged from Hunan Province accounts for 40% and 10.3% of the total discharge across China, respectively. Studies have illustrated that XR is the area most polluted by heavy metals in China, with the heavy metal pollution mainly derived from industrial manufacturing and refined mineral mining [21,59,60]. Therefore, the significantly higher concentration of Cd and As observed in the sediment of XR, compared with the other three rivers, indicates that As and Cd may be mainly produced by industrial wastewater and mineral mining processes. According to the   I g e o , EF, and RI values established, the studied sediment was not polluted by Cr, with Pb pollution absent to moderate. Therefore, Cr and Pb may be partly produced by natural sources, however, the distinct spatial distribution patterns indicate that these two metals may derive from different sources. Cr concentrations showed low spatial variation, which suggests a non-point agricultural origin. According to the Huan statistical Year Book (2017), 118,661 tons of pesticides were used in Hunan Province in 2017, with most of these pesticides containing metals including Cr. Thus, Cr may mainly originate from natural sources and agricultural activities [21]. Zn and Cu originate from both the sources of Cd/As and Cr. Atmospheric and river inflows transport Pb from industrial wastewater and sewage discharge [25,61].
This study comprehensively assessed the pollution status of heavy metals in the sediment of main tributaries of Dongting Lake. This provides a reference for aquatic environmental management of heavy metals in Dongting Lake drainage. However, further study is needed for a deeper understanding of the heavy metals in the sediment of studied rivers. Firstly, it is the bioavailability rather than the total concentration decides the toxicity of heavy metals. Therefore, further studies should be conducted on speciation of heavy metals in the sediments of these tributaries to confirm their toxicity. Secondly, although environmental factors of pH, organic matter, and Eh were mentioned in this study, no data were measured and no further correlation were analyzed between these factors and heavy metal concentrations. More studies should be conducted to make clear the relationship between environmental factors and heavy metal speciation in the sediment of the four rivers. Lastly, this study confirmed that heavy metals in the sediment of the four rivers are important sources of Dongting Lake. Deeper studies should be conducted to configure to what extent these heavy metals from the four rivers contribute to the Dongting Lake sediment.

5. Conclusions

The identification and quantification of heavy metal pollution in the sediment of tributaries in Dongting Lake is of great importance for the maintenance of a healthy ecosystem. Concentrations of the studied heavy metals exceeded the criteria values of UCC, US EPA, and the background value of the Dongting Lake sediment. The highest exceedance was Cd, which had concentration about 60-fold higher than the guideline values. The concentrations of the studied heavy metals were highest in XR, especially in the midstream and downstream regions. The PCA and correlation analysis indicates that Cd and As originated mainly from industrial wastewater and mineral mining; Cr originated from natural processes and agricultural activities; Zn and Cu may originate from both sources of Cd/As and Cr; and Pb was mainly from atmospheric deposition and river inflow transportation. According to the I g e o , EF, and RI assessment, the heavy metal pollution of the sediment was highest at XR, presenting considerable potential ecological risk. Cd was the main pollutant in the sediment of XR, which contributes significantly to the very high ecological risk level. Therefore, special attention should be paid to heavy metals in the sediment of XR, especially Cd pollution, in order to keep the whole ecosystem healthy. Furthermore, in this study, anthropogenic activity is the main reason for heavy metal pollution, thus, further field investigation should be conducted for the source identification, and then measures should be taken to control the pollutants from the source. This work provides basic information for the heavy metal distribution, source, and pollution status, and serves as a reference for heavy metal pollution management in the sediment of Dongting Lake area.

Supplementary Materials

Supplementary File 1

Author Contributions

J.X., Y.C., and X.W. conceived of the original outline for this study and designed the sampling points. J.L. and B.L. helped in the data processing and result analysis. L.Z. performed the analysis with constructive discussions. J.X. wrote the paper. All of the authors read and approved the final manuscript.

Funding

This research was funded by the STS (Science and Technology Service Network Initiative) Project of theChinese Academy of Sciences (KFJ-STS-ZDTP-011) and the Basic Work of Science and Technology (Grants 2012FY111800-03, 2013FY111802).

Acknowledgments

We thank Poyang Laboratory for the Wetland Ecosystem Research, and the Chinese Academy of Science for the assistance in the water samples collection.

Conflicts of Interest

The authors declare no conflict of interest.

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Figure 1. Study area and sampling locations in the four tributaries of Dongting Lake, China.
Figure 1. Study area and sampling locations in the four tributaries of Dongting Lake, China.
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Figure 2. Heavy metal concentrations in the sediment of the four studied rivers. XR—Xiangjiang River; ZR—Zishui River; YR—Yuanjiang River; LR—Lishui River.
Figure 2. Heavy metal concentrations in the sediment of the four studied rivers. XR—Xiangjiang River; ZR—Zishui River; YR—Yuanjiang River; LR—Lishui River.
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Figure 3. Heavy metal concentrations in different reaches of studied rivers (all metals in unit of mg/kg).
Figure 3. Heavy metal concentrations in different reaches of studied rivers (all metals in unit of mg/kg).
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Figure 4. Plot of the loading of the first two rotated principle components.
Figure 4. Plot of the loading of the first two rotated principle components.
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Table 1. The enrichment factor (EF), geo-accumulation index ( I g e o ), and risk index (RI) classes in relation to sediment quality.
Table 1. The enrichment factor (EF), geo-accumulation index ( I g e o ), and risk index (RI) classes in relation to sediment quality.
EF Class aSediment Quality I g e o Class bSediment Quality E r i Class Potential RiskRI Class cEcological Risk
EF < 1No enrichment<0Unpolluted E r i < 40LowRI < 150Low
1 ≤ EF < 3Minor enrichment0–1Unpolluted to moderately polluted40 ≤ E r i < 80Moderate150 ≤ RI < 300Moderate
3 ≤ EF < 5Moderate enrichment1–2Moderately polluted80 ≤ E r i < 160Considerable 300 ≤ RI < 600Considerable
5 ≤ EF < 10Moderately severe enrichment2–3Moderately to highly polluted160 ≤ E r i < 320HighRI ≥ 600Very high
10 ≤ EF < 25Very severe enrichment3–4Highly polluted E r i ≥ 320Very high
EF ≥ 25 Extremely Severe enrichment4–5Highly to very highly polluted
>5Very highly polluted
a Zahra et al. [9]; b Muller et al. [28]; c Hakanson. [29].
Table 2. Comparison of metals in sediment with different national and international guidelines and studies about rivers.
Table 2. Comparison of metals in sediment with different national and international guidelines and studies about rivers.
Studies and GuidlinesZn (mg/kg)Cr (mg/kg)Cu (mg/kg)As (mg/kg)Cd (mg/kg)Pb (mg/kg)Reference
Dongting Lake branches197 (32–576)66 (22–146)42 (13–106)38 (6.11–136)5.85 (0.41–34)71 (19–244)This study
Yangtze River (China)66.9134.6417.467.860.1530.47[30]
Yellow River (China)68.462.440.72.460.08515.2[31]
Liaohe River (China)50.2435.0617.829.881.210.57[16]
Korotoa River (Asia) 10976251.258[26]
Tajan River (Asia)19.7419.97 12.76 [32]
Tigris River (European)60.1–2396.628.4–163.411.2–5076.62.0–18.00.7–4.962.3–566.6[33]
Daube River (European)1876465.717.61.246.3[34]
Kafue River (Austrillia)75.336.7315.76.290.3514.8[35]
UCC713525 0.09820[36]
US EPA12143.431.69.80.9935.8[37]
TEL *12452.318.77.20.6830.2[38]
PEL *271160.4108.241.60.76112.2[38]
Background value of Dongting Lake sediment 83.34420.212.90.3323.3[39]
Note: * TEL represents threshold effects level; PEL represents the probable effects level. Adverse effects are expected to occur only rarely when the values of heavy metals are below the TEL; adverse biological effects can occasionally occur when the values are between the TEL and the PEL; adverse biological effects occur more frequently when the values exceed the PEL. TEL represents the concentration below which the adverse effects are expected to occur only rarely; PEL represents the concentration above which adverse effects are expected to occur frequently. UCC—upper continental crust; USEPA—United States Environmental Protection Agency.
Table 3. EF values of analyzed metals in river sediments. XR—Xiangjiang River; ZR—Zishui River; YR—Yuanjiang River; LR—Lishui River.
Table 3. EF values of analyzed metals in river sediments. XR—Xiangjiang River; ZR—Zishui River; YR—Yuanjiang River; LR—Lishui River.
RiversSectionZnCrCuAsCdPb
XRUP1.391.431.561.324.431.47
MID4.021.383.188.3354.263.89
DOWN4.881.472.666.3542.065.00
Average3.431.432.475.3333.583.45
ZRUP1.340.792.131.382.581.61
MID2.981.171.372.1710.342.24
DOWN1.601.241.612.5010.401.37
Average1.971.061.702.017.771.74
YRUP1.131.451.810.741.468.87
MID1.811.221.611.8317.831.45
DOWN1.541.251.322.057.801.95
Average1.491.301.581.549.034.09
LRUP0.660.950.880.6315.791.00
MID1.121.411.441.681.761.30
DOWN1.091.451.320.842.161.31
Average0.961.271.211.056.571.20
total average1.961.261.742.4814.242.62
Table 4. I g e o of the analyzed metals in the river sediment.
Table 4. I g e o of the analyzed metals in the river sediment.
RiversSectionZnCrCuAsCdPb
XRUpstream0.380.420.570.182.030.47
Midstream1.52−0.041.182.555.211.47
Downstream2.190.471.322.505.202.23
Average1.360.281.021.744.141.39
ZRUpstream0.13−0.650.690.181.020.40
Midstream1.00−0.29−0.100.522.850.66
Downstream0.400.020.401.033.090.17
Average0.51−0.300.330.572.320.41
YRUpstream−0.41−0.050.29−1.01−0.072.52
Midstream0.660.100.480.673.940.33
Downstream0.230.010.090.661.710.60
Average0.160.020.290.101.861.15
LRUpstream−1.31−0.82−0.80−1.182.21−0.52
Midstream−0.50−0.17−0.14−0.340.09−0.32
Downstream−0.55−0.14−0.27−0.940.44−0.28
Average−0.79−0.37−0.40−0.820.91−0.37
Total average0.31−0.090.310.402.310.64
Table 5. The potential ecological risk index of analyzed metals in river sediments.
Table 5. The potential ecological risk index of analyzed metals in river sediments.
RiversSectionERRI
ZnCrCuAsCdPb
XRUpper0.952.214.6819.2760.473.5091.08
Middle2.211.587.5175.61661.187.49755.57
Lower3.262.037.5774.51565.2111.74664.33
Average2.141.946.5956.46428.957.58503.66
ZRUpper0.780.965.0614.6732.653.2957.41
Middle1.491.222.9620.16109.823.98139.63
Lower0.941.494.0126.37126.792.81162.40
Average1.071.224.0120.4089.753.36119.81
YRUpper0.541.483.696.6514.3014.5441.19
Middle1.151.594.3420.96228.363.20259.59
Lower0.881.473.2321.4792.423.94123.42
Average0.861.513.7516.36111.697.23141.40
LRUpper0.320.941.835.77179.971.75190.58
Middle0.521.312.8214.7916.192.1337.77
Lower0.511.372.617.2920.362.0834.21
Average0.451.212.429.2872.181.9987.52
Total average1.131.474.1925.63175.645.04213.10
Table 6. Correlation of analyzed metals in river sediments.
Table 6. Correlation of analyzed metals in river sediments.
VariablesZnCrCuAsCdPb
Zn1
Cr0.5481
Cu0.7790.7451
As0.7720.1040.4331
Cd0.7850.1670.4950.9011
Pb0.3970.4560.3040.1920.1811
Note: The number in bold indicates correlation is significant at p < 0.05 level.
Table 7. Loading corresponding to the first two components for surface sediments of the four rivers.
Table 7. Loading corresponding to the first two components for surface sediments of the four rivers.
MetalsComponents
12
Zn0.7870.555
Cr0.0490.934
Cu0.4540.762
As0.9640.062
Cd0.9590.115
Pb0.0740.675
Eigenvalues3.5311.386
% total variance58.85423.092
% cumulative total variance58.85481.946
Note: significant factor loadings are bold faced.

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Xu, J.; Chen, Y.; Zheng, L.; Liu, B.; Liu, J.; Wang, X. Assessment of Heavy Metal Pollution in the Sediment of the Main Tributaries of Dongting Lake, China. Water 2018, 10, 1060. https://doi.org/10.3390/w10081060

AMA Style

Xu J, Chen Y, Zheng L, Liu B, Liu J, Wang X. Assessment of Heavy Metal Pollution in the Sediment of the Main Tributaries of Dongting Lake, China. Water. 2018; 10(8):1060. https://doi.org/10.3390/w10081060

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Xu, Jinying, Yuwei Chen, Lilin Zheng, Baogui Liu, Jinfu Liu, and Xiaolong Wang. 2018. "Assessment of Heavy Metal Pollution in the Sediment of the Main Tributaries of Dongting Lake, China" Water 10, no. 8: 1060. https://doi.org/10.3390/w10081060

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